FRINK Linked Data Fragments server

Matches in SemOpenAlex for { <https://semopenalex.org/work/W3007586096> ?p ?o ?g. }

• W3007586096 endingPage "104297" @default.
• W3007586096 startingPage "104297" @default.
• W3007586096 abstract "The ca. 1730 Ma Wollogorang Formation is a mixed carbonate-siliciclastic unit in the southern McArthur Basin of northern Australia. It is an exploration target for base metals and may be a petroleum source unit and unconventional reservoir. Facies analysis indicates that the Wollogorang Formation records deposition in supratidal to offshore environments. Lateral consistency in facies, thickness, and stratigraphic architecture suggests deposition on an east-west trending (present coordinates) epeiric platform. According to recent tectonic models for northern Australia, this epeiric platform likely deepened to the present-day east. The Wollogorang Formation comprises one second-order and five nested third-order sequences. Despite the unavailability of biostratigraphy and biofacies, and the general poor time control in Precambrian basins, we are able correlate third-order (i.e., our lowest rank) sequences over tens to hundreds of kilometers using high-resolution facies and petrophysical logs. As the distinction between stratigraphic sequences (related to shoreline shifts) and sedimentological bedsets (not related to shoreline shifts) becomes more difficult with decreasing hierarchical level, sedimentological, stratigraphic, paleontological, and mineralogical (including diagenetic) criteria were recently proposed to distinguish these cycles. Our study suggests that sedimentological and stratigraphic criteria are the most useful in Precambrian sequence stratigraphy. In contrast, paleontological criteria are irrelevant in Precambrian successions. Mineralogical (including diagenetic) criteria have not been tested in this study. In addition to further study these criteria, we suggest testing geochemical criteria, such as the enrichment of redox-sensitive trace elements and minor carbonate carbon isotope variation, to distinguish stratigraphic sequences from sedimentological bedsets." @default.
• W3007586096 created "2020-03-06" @default.
• W3007586096 creator A5005574367 @default.
• W3007586096 creator A5046466285 @default.
• W3007586096 creator A5079751043 @default.
• W3007586096 creator A5082530407 @default.
• W3007586096 creator A5082580478 @default.
• W3007586096 creator A5087721813 @default.
• W3007586096 date "2020-06-01" @default.
• W3007586096 modified "2023-10-06" @default.
• W3007586096 title "Sequence stratigraphy of the ca. 1730 Ma Wollogorang Formation, McArthur Basin, Australia" @default.
• W3007586096 cites W1629082400 @default.
• W3007586096 cites W1976131042 @default.
• W3007586096 cites W1977934505 @default.
• W3007586096 cites W1980270634 @default.
• W3007586096 cites W1981438127 @default.
• W3007586096 cites W1989164119 @default.
• W3007586096 cites W1996449743 @default.
• W3007586096 cites W1998556342 @default.
• W3007586096 cites W2000624053 @default.
• W3007586096 cites W2010527533 @default.
• W3007586096 cites W2015959750 @default.
• W3007586096 cites W2028319051 @default.
• W3007586096 cites W2029023074 @default.
• W3007586096 cites W2050016056 @default.
• W3007586096 cites W2050440902 @default.
• W3007586096 cites W2054561136 @default.
• W3007586096 cites W2055242142 @default.
• W3007586096 cites W2055748926 @default.
• W3007586096 cites W2058366574 @default.
• W3007586096 cites W2059981388 @default.
• W3007586096 cites W2061858157 @default.
• W3007586096 cites W2063352566 @default.
• W3007586096 cites W2067091950 @default.
• W3007586096 cites W2073071534 @default.
• W3007586096 cites W2077135172 @default.
• W3007586096 cites W2077493710 @default.
• W3007586096 cites W2080830021 @default.
• W3007586096 cites W2082070207 @default.
• W3007586096 cites W2091966944 @default.
• W3007586096 cites W2093879665 @default.
• W3007586096 cites W2094581504 @default.
• W3007586096 cites W2094740051 @default.
• W3007586096 cites W2098762071 @default.
• W3007586096 cites W2099208794 @default.
• W3007586096 cites W2100232434 @default.
• W3007586096 cites W2101608936 @default.
• W3007586096 cites W2151298887 @default.
• W3007586096 cites W2160804234 @default.
• W3007586096 cites W2281031690 @default.
• W3007586096 cites W2578032697 @default.
• W3007586096 cites W2586471818 @default.
• W3007586096 cites W2600398146 @default.
• W3007586096 cites W2612982774 @default.
• W3007586096 cites W2745744375 @default.
• W3007586096 cites W2773552765 @default.
• W3007586096 cites W2773771987 @default.
• W3007586096 cites W2790399336 @default.
• W3007586096 cites W2894810724 @default.
• W3007586096 cites W2900634359 @default.
• W3007586096 cites W2914258751 @default.
• W3007586096 cites W2942919097 @default.
• W3007586096 cites W2954966843 @default.
• W3007586096 cites W2981558207 @default.
• W3007586096 doi "https://doi.org/10.1016/j.marpetgeo.2020.104297" @default.
• W3007586096 hasPublicationYear "2020" @default.
• W3007586096 type Work @default.
• W3007586096 sameAs 3007586096 @default.
• W3007586096 citedByCount "9" @default.
• W3007586096 countsByYear W30075860962020 @default.
• W3007586096 countsByYear W30075860962021 @default.
• W3007586096 countsByYear W30075860962022 @default.
• W3007586096 countsByYear W30075860962023 @default.
• W3007586096 crossrefType "journal-article" @default.
• W3007586096 hasAuthorship W3007586096A5005574367 @default.
• W3007586096 hasAuthorship W3007586096A5046466285 @default.
• W3007586096 hasAuthorship W3007586096A5079751043 @default.
• W3007586096 hasAuthorship W3007586096A5082530407 @default.
• W3007586096 hasAuthorship W3007586096A5082580478 @default.
• W3007586096 hasAuthorship W3007586096A5087721813 @default.
• W3007586096 hasConcept C109007969 @default.
• W3007586096 hasConcept C109281948 @default.
• W3007586096 hasConcept C127313418 @default.
• W3007586096 hasConcept C130452526 @default.
• W3007586096 hasConcept C146588470 @default.
• W3007586096 hasConcept C151730666 @default.
• W3007586096 hasConcept C158787203 @default.
• W3007586096 hasConcept C173776410 @default.
• W3007586096 hasConcept C185059815 @default.
• W3007586096 hasConcept C18903297 @default.
• W3007586096 hasConcept C190890723 @default.
• W3007586096 hasConcept C2776340010 @default.
• W3007586096 hasConcept C42907665 @default.
• W3007586096 hasConcept C48258643 @default.
• W3007586096 hasConcept C61721801 @default.
• W3007586096 hasConcept C77928131 @default.
• W3007586096 hasConcept C86803240 @default.
• W3007586096 hasConcept C93257316 @default.

• next